Introduction to the Shiniushan Geopark: The Shiniushan Geopark is the product of the last sedimentary volcanic eruption cycle in the Late Cretaceous in Fujian. It represents the final end of the late Mesozoic volcanic activity in the southeastern mainland of China. The huge height difference of 1,500 meters makes the Shiniushan Mountains It has become a natural three-dimensional model of a volcano, with complete rock exposure and obvious lithological zoning, reflecting the complete geological evolution process from volcanic eruption to collapse to resurrection uplift. Natural museum. After long-term weathering and water erosion, the mountain has formed today's unique geological landscape, which has extremely high scientific research and ornamental value.